Mantle Source and Metasomatic Agent of Olivine Nephelinites: Insights into Olivine Geochemistry, Oxygen Isotopes and Whole-Rock Os Isotopes.
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| Title: | Mantle Source and Metasomatic Agent of Olivine Nephelinites: Insights into Olivine Geochemistry, Oxygen Isotopes and Whole-Rock Os Isotopes. |
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| Authors: | Wang, Changhong1 (AUTHOR), Wang, Jie1 (AUTHOR), Velásquez-Ruiz, Felipe2 (AUTHOR), Conticelli, Sandro3 (AUTHOR), Molina, José F4 (AUTHOR), Zhang, Zhaochong1 (AUTHOR), Wang, Yujian1 (AUTHOR), Xie, Qiuhong5 (AUTHOR), Bo, Hongze6 (AUTHOR), Krmíček, Lukáš7 (AUTHOR) |
| Source: | Journal of Petrology. Apr2026, Vol. 67 Issue 4, p1-15. 15p. |
| Subject Terms: | *Metasomatism, *Osmium isotopes, *Geochemistry, *Alkalic igneous rocks, *Oxygen isotopes, *Ultrabasic rocks, *Earth's mantle |
| Geographic Terms: | Qinling Mountains (China), China |
| Abstract: | Nephelinites are a distinctive group of silica-undersaturated, strongly alkaline ultrabasic volcanic rocks that are occasionally associated with carbonatites. Their genesis has been attributed to the melting of a mantle source enriched by either recycled crustal materials or other metasomatic agents. This study investigates olivine nephelinites and constrains their mantle source from the West Qinling orogen, Central China—a locality noted for its unique occurrence of rocks previously classified as kamafugites or melilitites in China. Olivines in these rocks are categorized into Group I mantle xenocrysts (Fo89–92) and Group II magmatic crystals (Fo81–88). In situ δ18O values of the Group II magmatic olivines (5.04 ± 0.25‰; 1σ, n = 67) are slightly lower than those of Group I mantle xenocrysts (5.26 ± 0.20‰, 1σ, n = 199). Measured 187Os/188Os ratios for these nephelinites are moderately to highly radiogenic (0.138–0.682), with age-corrected γOs values varying from +6.57 to +409. Magmatic olivines with elevated 100 × Mn/Fe (mean = 1.65), 100 × Ni/Mg (mean = 0.70) and high 100 × Ca/Fe (mean = 2.33) ratios fingerprint a metasomatized mantle peridotite source. Binary mixing indicates that the observed radiogenic Os isotopes can be explained by the incorporation of <30% melts/fluids derived from a subducted oceanic slab. Our findings suggest that mantle metasomatism, driven by recycled oceanic slabs, played a major role in alkaline enrichment observed in the West Qinling magmas and may provide new insights into the crust–mantle interaction. [ABSTRACT FROM AUTHOR] |
| Database: | Energy & Power Source |
| FullText | Text: Availability: 0 |
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| Header | DbId: enr DbLabel: Energy & Power Source An: 194374367 AccessLevel: 6 PubType: Academic Journal PubTypeId: academicJournal PreciseRelevancyScore: 0 |
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| Items | – Name: Title Label: Title Group: Ti Data: Mantle Source and Metasomatic Agent of Olivine Nephelinites: Insights into Olivine Geochemistry, Oxygen Isotopes and Whole-Rock Os Isotopes. – Name: Author Label: Authors Group: Au Data: <searchLink fieldCode="AR" term="%22Wang%2C+Changhong%22">Wang, Changhong</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Wang%2C+Jie%22">Wang, Jie</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Velásquez-Ruiz%2C+Felipe%22">Velásquez-Ruiz, Felipe</searchLink><relatesTo>2</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Conticelli%2C+Sandro%22">Conticelli, Sandro</searchLink><relatesTo>3</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Molina%2C+José+F%22">Molina, José F</searchLink><relatesTo>4</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Zhang%2C+Zhaochong%22">Zhang, Zhaochong</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Wang%2C+Yujian%22">Wang, Yujian</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Xie%2C+Qiuhong%22">Xie, Qiuhong</searchLink><relatesTo>5</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Bo%2C+Hongze%22">Bo, Hongze</searchLink><relatesTo>6</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Krmíček%2C+Lukáš%22">Krmíček, Lukáš</searchLink><relatesTo>7</relatesTo> (AUTHOR) – Name: TitleSource Label: Source Group: Src Data: <searchLink fieldCode="JN" term="%22Journal+of+Petrology%22">Journal of Petrology</searchLink>. Apr2026, Vol. 67 Issue 4, p1-15. 15p. – Name: Subject Label: Subject Terms Group: Su Data: *<searchLink fieldCode="DE" term="%22Metasomatism%22">Metasomatism</searchLink><br />*<searchLink fieldCode="DE" term="%22Osmium+isotopes%22">Osmium isotopes</searchLink><br />*<searchLink fieldCode="DE" term="%22Geochemistry%22">Geochemistry</searchLink><br />*<searchLink fieldCode="DE" term="%22Alkalic+igneous+rocks%22">Alkalic igneous rocks</searchLink><br />*<searchLink fieldCode="DE" term="%22Oxygen+isotopes%22">Oxygen isotopes</searchLink><br />*<searchLink fieldCode="DE" term="%22Ultrabasic+rocks%22">Ultrabasic rocks</searchLink><br />*<searchLink fieldCode="DE" term="%22Earth's+mantle%22">Earth's mantle</searchLink> – Name: SubjectGeographic Label: Geographic Terms Group: Su Data: <searchLink fieldCode="DE" term="%22Qinling+Mountains+%28China%29%22">Qinling Mountains (China)</searchLink><br /><searchLink fieldCode="DE" term="%22China%22">China</searchLink> – Name: Abstract Label: Abstract Group: Ab Data: Nephelinites are a distinctive group of silica-undersaturated, strongly alkaline ultrabasic volcanic rocks that are occasionally associated with carbonatites. Their genesis has been attributed to the melting of a mantle source enriched by either recycled crustal materials or other metasomatic agents. This study investigates olivine nephelinites and constrains their mantle source from the West Qinling orogen, Central China—a locality noted for its unique occurrence of rocks previously classified as kamafugites or melilitites in China. Olivines in these rocks are categorized into Group I mantle xenocrysts (Fo89–92) and Group II magmatic crystals (Fo81–88). In situ δ18O values of the Group II magmatic olivines (5.04 ± 0.25‰; 1σ, n = 67) are slightly lower than those of Group I mantle xenocrysts (5.26 ± 0.20‰, 1σ, n = 199). Measured 187Os/188Os ratios for these nephelinites are moderately to highly radiogenic (0.138–0.682), with age-corrected γOs values varying from +6.57 to +409. Magmatic olivines with elevated 100 × Mn/Fe (mean = 1.65), 100 × Ni/Mg (mean = 0.70) and high 100 × Ca/Fe (mean = 2.33) ratios fingerprint a metasomatized mantle peridotite source. Binary mixing indicates that the observed radiogenic Os isotopes can be explained by the incorporation of <30% melts/fluids derived from a subducted oceanic slab. Our findings suggest that mantle metasomatism, driven by recycled oceanic slabs, played a major role in alkaline enrichment observed in the West Qinling magmas and may provide new insights into the crust–mantle interaction. [ABSTRACT FROM AUTHOR] |
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| RecordInfo | BibRecord: BibEntity: Identifiers: – Type: doi Value: 10.1093/petrology/egag031 Languages: – Code: eng Text: English PhysicalDescription: Pagination: PageCount: 15 StartPage: 1 Subjects: – SubjectFull: Metasomatism Type: general – SubjectFull: Osmium isotopes Type: general – SubjectFull: Geochemistry Type: general – SubjectFull: Alkalic igneous rocks Type: general – SubjectFull: Oxygen isotopes Type: general – SubjectFull: Ultrabasic rocks Type: general – SubjectFull: Earth's mantle Type: general – SubjectFull: Qinling Mountains (China) Type: general – SubjectFull: China Type: general Titles: – TitleFull: Mantle Source and Metasomatic Agent of Olivine Nephelinites: Insights into Olivine Geochemistry, Oxygen Isotopes and Whole-Rock Os Isotopes. Type: main BibRelationships: HasContributorRelationships: – PersonEntity: Name: NameFull: Wang, Changhong – PersonEntity: Name: NameFull: Wang, Jie – PersonEntity: Name: NameFull: Velásquez-Ruiz, Felipe – PersonEntity: Name: NameFull: Conticelli, Sandro – PersonEntity: Name: NameFull: Molina, José F – PersonEntity: Name: NameFull: Zhang, Zhaochong – PersonEntity: Name: NameFull: Wang, Yujian – PersonEntity: Name: NameFull: Xie, Qiuhong – PersonEntity: Name: NameFull: Bo, Hongze – PersonEntity: Name: NameFull: Krmíček, Lukáš IsPartOfRelationships: – BibEntity: Dates: – D: 01 M: 04 Text: Apr2026 Type: published Y: 2026 Identifiers: – Type: issn-print Value: 00223530 Numbering: – Type: volume Value: 67 – Type: issue Value: 4 Titles: – TitleFull: Journal of Petrology Type: main |
| ResultId | 1 |